• 자원환경지질
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• 제31권4호
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• pp.297-310
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• 1998

Geochemical characteristics of environmental toxic elements at the Narim mine area were investigated on the basis of major, minor, rare earth element geochemistry and mineralogy. Ratios of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in soils and sediments range from 11.57 to 22.21 and from 1.86 to 3.93, and are partly negative and positive correlation against $SiO_2/Al_2O_3$ (3.41 to 4.78), respectively. These suggested that sediment source of host granitic gneiss could be due to rocks of high grade metamorphism originated by sedimentary rocks. Characteristics of some trace and rare earth elements of V/Ni (0.33 to 1.95), Ni/Co (2.00 to 6.50), Zr/Hf (11.27 to 53.10), La/Ce (0.44 to 0.55), Th/Yb (4.07 to 7.14), La/Th (2.35 to 3.93), $La_N/Yb_N$ (6.58 to 13.67), Co/Th (0.63 to 2.68), La/Sc (3.29 to 5.94) and Sc/Th (0.49 to 1.00) are revealed a narrow range and homogeneous compositions may be explained by simple source lithology. Major elements in all samples are enriched $Al_2O_3$, MgO, $TiO_2$ and LOI, especially $Fe_2O_3$ (mean=7.36 wt.%) in sediments than the composition of host granitic gneiss. The average enrichment indices of major and rare earth elements from the mining drainage are 2.05 and 2.91 of the sediments and are 2.02 and 2.60 of the soils, normalizing by composition of host granitic gneiss, respectively. Average composition (ppm) of minor and/or environmental toxic elements in sediments and soils are Ag=14 and 1, As=199 and 14, Cd=22 and 1, Cu=215 and 42, Pb=1770 and 65, Sb=18 and 3, Zn=3333 and 170, respectively, and extremely high concentrations are found in the subsurface sediments near the ore dump. Environmental toxic elements were strongly enriched in all samples, especially As, Cd, Cu, Pb, Sb and Zn. The level of enrichment was very severe in mining drainage sediments, while it was not so great in the soils. Based on the EPA value, enrichment index of toxic elements is 8.63 of mining drainage sediments and 0.54 of soils on the mining drainage. Mineral composition of soils and sediments near the mining area were partly variable being composed of quartz, mica, feldspar, amphibole, chlorite and clay minerals. From the gravity separated mineralogy, soils and sediments are composed of some pyrite, arsenopyrite, chalcopyrite, sphalerite, galena, goethite and various hydroxide minerals.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2011년도 추계학술대회 초록집
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• pp.100-100
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• 2011

Nanomaterial architecture with highly ordered, vertically oriented $TiO_2$ nanotube arrays shows a good promise for diverse technological applications. As inspired from the literature reports that Nickel modification can improve the photocatalytic activity of $TiO_2$, it was planned to coat Ni into the $TiO_2$ matrix. In this study, first $TiO_2$ nanotubes(TiNTs) were prepared by anodization (60V,3min) in HF-free aqueous electrolyte on ultrasonically cleaned polished titanium sheet substrates ($1{\times}7cm^2$). The typical thickness of the sintered TiNT ($500^{\circ}C$for10min) was ~1 micronas confirmed from the FESEM study. In the next part, as-anodized and sintered TiNT/Ti photoanodes were used to coat Ni by AC electrodeposition from aqueous 0.1M nickel sulphate solution. During AC electrodeposition, conditions such as 1V DC offset voltage, 9V amplitude (peak-to-peak) and 750 Hz frequency were fixed constant and the deposition time was varied as 0.5 min, 1 min, 2 min and 10 min. The photoelectrochemical performance of pristine and Ni modified TiNT/Ti photoanodes was measured in 1N NaOH electrolyte under 1 SUN illumination in the potential range of -1V and 1.2V versus Ag/AgCl reference electrode. The photocurrent performance of TiNT/Ti photoanode decreased upon Ni modification and the results were confirmed after repeated experiments. This suggests us that Ni modification inhibits the photoelectrochemical performance of $TiO_2$ nanotubes.

• 한국자기학회지
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• 제10권5호
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• pp.220-224
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• 2000

Co-페라이트 CoF $e_2$ $O_4$에서 Fe 이온의 미량을 Co와 Ti 이온으로 치환시킨 시료인 $Co_{1+x}$/F $e_{2-}$2x// $Ti_{x}$ $O_4$(0.00$\leq$x$\leq$0.10)을 sol-gel방법으로 제조하여 Co와 Ti이온의 치환에 따른 결정학적 및 자기적 특성의 변화를 밝히기 위하여 x-선 회절기, Mossbauer분광기 , 진동자력계 등을 이용한 연구를 하였다. 결정 구조는 전체 조성비 범위에서 spinel임을 알 수 있었으며, 격자 상수 값은 Co-T리 치환량이 증가함에 따라 x = 0.00때 8.383 $\AA$에서 x = 0.l0때 8.397 $\AA$으로 선형적으로 증가하였다. 입자의 크기도 Co-Ti 치환량이 증가함에 따라 x = 0.00때 49.7 nm에서 x = 0.10때 46.6 nm로 감소하여 세라믹제조 방법에 비하여 매우 작게 나타났다. Mossbauer spectrum은 상온에서 F $e^{3+}$ 가 A와 B 자리에 위치하여 나타나는 한세트의 육중선이 중첩된 모양이었는데, Co-Ti의 치환량 증가에 따라 A자리의 초미세 자기장 값은 거의 일정하였으나 B자리의 값은 감소하였다. 이성질체 이동값과 사중극자 분열값은 거의 일정하였다. $Co_{1+x}$F $e_{2-}$2x/ $Ti_{x}$ $O_4$ 시료에서 포화자화는 x = 0.00때 77.1 emu/g에서 x = 0.10때 61.7 emu/g로 선형적으로 서서히 감소하고, 보자력은 x = 0.00때 545.0 Oe에서 x = 0.10때 327.0 Oe로 급격히 감소하였다.하였다.다.

• 한국분말재료학회지
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• 제13권5호
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• pp.327-335
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• 2006

In the development of new hydrogen absorbing materials for a next generation of metal hydride electrodes for rechargeable batteries, metastable Mg-Ni-based compounds find currently special attention. Amor phous-nanocrystalline $Mg_{63}Ni_{30}Y_7$ and $Mg_{50}Ni_{30}Y_{20}$ alloys were produced by mechanical alloying and melt-spinning and characterized by means of XRD, TEM and DSC. On basis of mechanically alloyed Mg-Ni-Y powders, complex hydride electrodes were fabricated and their electrochemical behaviour in 6M KOH (pH=14,8) was investigated. The electrodes made from $Mg_{63}Ni_{30}Y_7$ powders, which were prepared under use of a SPEX shaker mill, with a major fraction of nanocrystalline phase reveal a higher electrochemical activity far hydrogen reduction and a higher maximum discharge capacity (247 mAh/g) than the electrodes from alloy powder with predominantly amorphous microstructure (216 mAh/g) obtained when using a Retsch planetary ball mill at low temperatures. Those discharge capacities are higher that those fur nanocrystalline $Mg_2Ni$ electrodes. However, the cyclic stability of those alloy powder electrodes was low. Therefore, fundamental stability studies were performed on $Mg_{63}Ni_{30}Y_7$ and $Mg_{50}Ni_{30}Y_{20}$ ribbon samples in the as-quenched state and after cathodic hydrogen charging by means of anodic and cathodic polarisation measurements. Gradual oxidation and dissolution of nickel governs the anodic behaviour before a passive state is attained. A stabilizing effect of higher fractions of yttrium in the alloy on the passivation was detected. During the cathodic hydrogen charging process the alloys exhibit a change in the surface state chemistry, i.e. an enrichment of nickel-species, causing preferential oxidation and dissolution during subsequent anodization. The effect of chemical pre-treatments in 1% HF and in $10\;mg/l\;YCl_3/1%\;H_2O_2$ solution on the surface degradation processes was investigated. A HF treatment can improve their anodic passivation behavior by inhibiting a preferential nickel oxidation-dissolution at low polarisation, whereas a $YCl_3/H_2O_2$ treatment has the opposite effect. Both pre-treatment methods lead to an enhancement of cathodically induced surface degradation processes.

• Journal of Magnetics
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• 제12권4호
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• pp.137-140
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• 2007

We have studied the temperature dependent magnetic properties and crystalline phase transitionn in small amount Fe doped nickel chromite. The Crystalline structure of $NiCr_{1.7}Fe_{0.3}O_4$ is spinel cubic (Fd-3m) structure with a lattice constant $a_0=8.317\AA$ at room temperature. The magnetic $N\acute{e}el$ temperature $(T_N)$ of the Fe doped nickel chromite sample is determined to be 250 K. The $M\ddot{o}ssbauer$ spectra exhibit that there are two magnetic phases with the two different sites for the $Cr^{3+}$ ions. The spectrum at 4.2 K is fitted to two magnetic components of the magnetic hyperfine fields $H_{hf}=496$ and 485 kOe. From the spectrum at 295 K, the electric quadrupole splittings are observed with large values of 0.49 and 0.50 mm/s, respectively. The values of the isomer shifts at all temperature ranges show that the Fe ions are ferric states. We are suggested that the dynamic Jahn-Teller distortion and anisotropic magnetic relaxation effects due to the crystalline phase transition.

• 암석학회지
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• 제7권2호
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• pp.111-131
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• 1998

오대산편마암복합제의 미그미타이트질편마암내에는 규암, 앰피볼라이트, 대리암들이 협재되어 있으며 미그마타이트질편마암과 부정합적인 관계를 보이는 구룡층군 내에도 앰피볼라이트들이 나타난다. 기존 연구자들은 대리암과 접하고 있는 앰피볼라이트를 이질-탄산염질 기원물의 변성교대작용의 결과로 인식하고 있었으나 본 연구에서는 모두 화성기원으로 해석하였다. 앰피볼라이트의 $SiO_2$ 함량은 45.9~52.7 wt%로 현무암질에 해당한다. MgO의 함량은 비교적 좁은 범위(4.6~6.87 wt%)를 보이며 이를 이용한 분화정도를 살펴보면 MgO의 감소에 따라 $TiO_2, P_2O_5$, Hf, Zr은 감소하고 Cr과 Ni은 증가한다. 이러한 현상은 근원암인 현무암질 마그마에서 감람석 또는 휘석을 정출하는 분별정출작용의 결과이다. 희통류 성분은 LREE과 HREE 간의 변화폭이 작고 완만하다. $Eu/Eu^*$는 0.83~1.19로 Eu 이상치가 적어 사장석의 분별정출작용의 영향이 적었음을 지시하며 석류석을 함유하고 있는 앰피볼라이트는 HREE가 부화되는 경향을 보인다. 염기성마그마의 지구조 환경을 판별하는 여러 판별그림에 적용한 결과, 연구지역의 앰피볼라이트는 대륙판 열곡환경으리 지시하는 솔리아이트계열의 현무암질 마그마에서 유래되었음을 보여준다. 앰피볼라이트를 형성하는 변성작용을 알아보기 위해 석류석-각섬석 지온계와 석류석-각섬석-사장석 지온계를 이용하여 변성온도를 측정하였다. 앰피볼라이트의 최대 변성온도는 $788~870^{\circ}C$에 해당하며 북동쪽으로 가면서 변성온도가 감소한다. 이들 온도는 변성이질암에서 보고된 온도에 비하여 다소 높은 온도이나 변성정도가 서측에서 동측으로 가면서 감소하는 경향은 일치한다. 변성압력은 석류석-각섬석-사장석 지압계를 이용하여 측정한 결과 4~5 kb의 압력을 가진다. 그러나 석류석내에 포획되어 있는 사장석-티탄철석을 이용한 지압은 $700^{\circ}C$의 온도에 대해 8 kb 이상의 압력환경을 거쳤음을 지시한다. 시료 84의 석류석은 중심부에 균질한 조성을 거친후 점진적으로 그로슐라 함량은 감소하고 파이로프 함량은 증가하는 온도의 증가와 압력의 감소를 지시하는 벨형태의 누대구조를 보이고 있다. 이는 앰피볼라이트도 변성이질암과 마찬가지로 시계방향의 압력-온도-시간 경로를 거쳤음을 지시한다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2010년도 하계학술대회 논문집
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• pp.11-11
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• 2010

Thin-film-transistors (TFTs) that can be deposited at low temperature have recently attracted lots of applications such as sensors, solar cell and displays, because of the great flexible electronics and transparent. Transparent and flexible transistors are being required that high mobility and large-area uniformity at low temperature [1]. But, unfortunately most of TFT structures are used to be $SiO_2$ as gate dielectric layer. The $SiO_2$ has disadvantaged that it is required to high driving voltage to achieve the same operating efficiency compared with other high-k materials and its thickness is thicker than high-k materials [2]. To solve this problem, we find lots of high-k materials as $HfO_2$, $ZrO_2$, $SiN_x$, $TiO_2$, $Al_2O_3$. Among the High-k materials, $Al_2O_3$ is one of the outstanding materials due to its properties are high dielectric constant ( ~9 ), relatively low leakage current, wide bandgap ( 8.7 eV ) and good device stability. For the realization of flexible displays, all processes should be performed at very low temperatures, but low temperature $Al_2O_3$ grown by sputtering showed deteriorated electrical performance. Further decrease in growth temperature induces a high density of charge traps in the gate oxide/channel. This study investigated the effect of growth temperatures of ALD grown $Al_2O_3$ layers on the TFT device performance. The ALD deposition showed high conformal and defect-free dielectric layers at low temperature compared with other deposition equipments [2]. After ITO was wet-chemically etched with HCl : $HNO_3$ = 3:1, $Al_2O_3$ layer was deposited by ALD at various growth temperatures or lift-off process. Amorphous InGaZnO channel layers were deposited by rf magnetron sputtering at a working pressure of 3 mTorr and $O_2$/Ar (1/29 sccm). The electrodes were formed with electron-beam evaporated Ti (30 nm) and Au (70 nm) bilayer. The TFT devices were heat-treated in a furnace at $300^{\circ}C$ and nitrogen atmosphere for 1 hour by rapid thermal treatment. The electrical properties of the oxide TFTs were measured using semiconductor parameter analyzer (4145B), and LCR meter.

• 한국재료학회:학술대회논문집
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• 한국재료학회 1992년도 춘계학술발표회
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• pp.26-27
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• 1992

반도체 기억소자 contact hole의 선택적 충진의 최적 조건을 연구하기 위하여 무전해Ni도금방법을 채택하여 실리콘의 활성화와 선택적 도금의 공정조건이 Contact Hole 도금피막의 제반 특성에 미치는 영향을 조사하였다. p형 실리콘 100 소지 표면의 활성화 처리는 RCA처리에 의해 먼저 표면을 세척한 다음 온도, PdCl$_2$농도, 시간. 교반의 영향을 조사하였다 전처리의 최적조건은 7$0^{\circ}C$, 0.5M HF, ImM PdCl$_2$, 2mM EDTA, 90second이었다. 무전해도금은 NiS0$_4$.6$H_2O$를 DMAB를 환원제로 하여 온도, DMAB 농도, pH, 도금시간의 영향을 조사하였다. 무전해 도금 피막은 비교적 우수한 접촉저 항을 나타냈다. 1$\mu$m의 도금막을 얻는 데 본 실험조건에서 DMAB의 농도가 8mM일 때 30 분이 소요되었다. 도금막의 표면은 온도가 낮을수록 pH가 높을수록 평활하였고,특히 온도 6$0^{\circ}C$와 pH6.8에서 가장 우수하였다. 미세경도는 600Hv 정도였으며, 결정립의 크기 가 증가할수록 저항과 미세경도가 감소하였다.

• 광물과 암석
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• 제33권2호
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• pp.115-127
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• 2020

운산 금 광상은 한반도의 3대(대유동 광상, 광양 광상) 금 광상중의 하나이었다. 이 광상 주변지질은 선캠브리아기의 변성퇴적암류와 중생대의 반상화강암으로 구성된다. 이 광상은 선캠브리아기의 변성퇴적암류와 중생대의 반상화강암내에 발달된 단층대를 따라 충진한 함 금 석영맥 광상으로 조산형 금 광상에 해당된다. 이 광상의 석영맥은 광물조합에 따라 1)방연석-석영맥형, 2)자류철석-석영맥형, 3)황철석-석영맥형, 4)페크마틱 석영맥형, 5)백운모-석영맥형 및 6)단순석영맥형으로 분류된다. 연구된 석영맥은 황철석-석영맥형이며 견운모화작용, 녹니석화작용 및 규화작용이 관찰된다. 이 석영맥은 백색 석영, 백색 운모, 녹니석, 황철석, 금홍석, 방해석, 모나자이트, 저어콘 및 인회석 등이 산출된다. 금홍석은 엽리상 석영맥내 유색대에서 자형내지 중립질 입단으로 어두운 금홍석과 밝은 금홍석으로 산출된다. 금홍석의 화학조성은 89.69~98.71 wt.% (TiO₂), 0.25~7.04 wt.% (WO₃), 0.30~2.56 wt.% (FeO), 0.00~1.71 wt.% (Nb₂O₅), 0.17~0.35 wt.% (HfO₂), 0.00~0.30 wt.% (V₂O₃), 0.00~0.35 wt.% (Cr₂O₃) 및 0.04~0.25 wt.% (Al₂O₃)으로 밝은 금홍석이 어두운 금홍석보다 WO₃, Nb₂O₅ 및 FeO 원소들의 함량이 높게 산출되며 서로 다른 시기에 형성된 것으로 생각된다. 어두운 금홍석과 밝은 금홍석내 미량원소들은 어두운 금홍석 [(V³⁺, Cr³⁺) + (Nb⁵⁺, Sb⁵⁺) ↔ 2Ti⁴⁺, 4Cr³⁺ (or 2W⁶⁺) ↔ 3Ti⁴⁺ (W⁶⁺ ↔ 2Cr³⁺), V⁴⁺ ↔ Ti⁴⁺], 밝은 금홍석 [2Fe³⁺ + W⁶⁺ ↔ 3Ti⁴⁺, 3Fe²⁺ + W⁶⁺ ↔ Ti⁴⁺ + (V³⁺, Al³⁺, Cr³⁺) +Nb⁵⁺]로써 치환관계가 있었다. 이들 자료를 근거로, 어두운 금홍석은 광역변성작용 동안 모암광물들의 변질 시 광물내 존재했던 V³⁺, V⁴⁺, Cr³⁺, Nb⁵⁺, Sb⁵⁺, W⁶⁺과 같은 양이온들의 재 농집에 의해 형성되었으나 밝은 금홍석은 ductile shear 시 높은 함량의 Fe²⁺ 및 W⁶⁺ 양이온들을 함유한 열수용액의 유입에 따른 어두운 금홍석과 반응에 의해 어두운 금홍석에 존재하였던 V³⁺, V⁴⁺, Al³⁺, Cr³⁺ 및 Nb⁵⁺과 같은 양이온들의 재 농집에 의해 형성된 것으로 생각된다.

• Nutrition Research and Practice
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• 제10권3호
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• pp.265-273
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• 2016

BACKGROUND/OBJECTIVES: The inhibitory effect of Hijikia fusiforme (HF) extracts on degenerative osteoarthritis was examined in primary cultured rat cartilage cells and a monosodium iodoacetate (MIA)-induced osteoarthritis rat model. MATERIALS/METHODS: In vitro, cell survival and the expression of matrix metalloproteinases (MMPs), collagen type I, collagen type II, aggrecan, and tissue inhibitor of metalloproteinases (TIMPs) was measured after $H_2O_2$ ($800{\mu}M$, 2 hr) treatment in primary chondrocytes. In vivo animal study, osteoarthritis was induced by intra-articular injection of MIA into knee joints of rats, and then RH500, HFE250 and HFE500 were administered orally once a day for 28 days. To determine the anti-inflammatory effects of HFE, nitric oxide (NO), prostaglandin $E_2$ ($PGE_2$) expression were measured. In addition, real-time PCR was performed to measure the genetic expression of MMPs, collagen type I, collagen type II, aggrecan, and TIMPs. RESULTS: In the in vitro assay, cell survival after $H_2O_2$ treatment was increased by HFE extract (20% EtOH). In addition, anabolic factors (genetic expression of collagen type I, II, and aggrecan) were increased by HFE extract (20% EtOH). However, the genetic expression of MMP-3 and 7, known as catabolic factors were significantly inhibited by treatment with HFE extract (20% EtOH). In the in vivo assay, anabolic factors (genetic expression of collagen type I, II, aggrecan, and TIMPs) were increased by oral administration of HFE extract. However, the genetic expression of MMP-3 and 7, known as catabolic factors, and production of NO and $PGE_2$ were significantly inhibited by treatment with oral administration of HFE extract. CONCLUSION: HFE extract inhibited articular cartilage degeneration through preventing extracellular matrix degradation and chondrocyte injury.